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National Geologic Map Database
Geologic Unit: Laurel
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Map showing publication footprint
  • Usage in publication:
    • Laurel migmatite
  • Modifications:
    • Named
  • Dominant lithology:
    • Migmatite
    • Gneiss
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Cloos, Ernst, and Broedel, C.H., 1940, Geologic map of Howard County and adjacent parts of Montgomery and Baltimore Counties [Maryland]: Maryland Geological Survey County Geologic Map, 1 sheet, scale 1:62,500


Summary:

Name Laurel migmatite introduced on this map for granitized schist mixed with impure granite mapped in vicinity of Laurel, Prince Georges Co., MD, 17 mi southwest of Baltimore. Described as muscovite and biotite granite. Age unknown.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Laurel gneiss, pseudomigmatite
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Chapman, R.W., 1942, "Pseudomigmatite" in the Piedmont of Maryland: Geological Society of America Bulletin, v. 53, no. 9, p. 1299-1328.


Summary:

Although Laurel gneiss resembles a true migmatite, term pseudomigmatite is more appropriate. Gneiss is bounded on north by Guilford granite and Wissahickon formation, on northeast by gabbro, on east by Cretaceous gravels, on south by gneiss, and on west by the Wissahickon.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Laurel gneiss
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Cloos, Ernst, and Cooke, C.W., 1953, Geologic map of Montgomery County [Maryland] and District of Columbia: Maryland Geological Survey County Geologic Map, 1 sheet, scale 1:62,500


Summary:

Mapped in Montgomery Co. as Laurel gneiss. Very similar to Sykesville formation and possibly its equivalent southwest of Woodstock anticlinorium.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Laurel Formation
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Hopson, C.A., 1964, The crystalline rocks of Howard and Montgomery Counties: Maryland Geological Survey County Report, 337 p., Reprinted from Cloos, Ernst, and others, "Geology of Howard and Montgomery Counties," p. 27-215


Summary:

Unit mapped as Laurel Formation. Part of Glenarm series. Age is Late Precambrian or Cambrian.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Laurel lithofacies
  • Modifications:
    • Revised
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Southwick, D.L., and Fisher, G.W., 1967, Revision of stratigraphic nomenclature of the Glenarm series in Maryland: Maryland Geological Survey Report of Investigations, no. 6, 19 p.


Summary:

Laurel included in Wissahickon Formation as a lithofacies. Age given as Late Precambrian(?).

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Laurel Formation*
  • Modifications:
    • Overview
  • Dominant lithology:
    • Meta-arenite
    • Schist
    • Amphibolite
  • AAPG geologic province:
    • Piedmont-Blue Ridge province
Publication:

Fleming, A.H., Drake, A.A., Jr., and McCartan, Lucy, 1994, Geologic map of the Washington West quadrangle, District of Columbia, Montgomery and Prince Georges Counties, Maryland, and Arlington and Fairfax Counties, Virginia: U.S. Geological Survey Geologic Quadrangle Map, GQ-1748, 1 sheet, scale 1:24,000 [http://ngmdb.usgs.gov/Prodesc/proddesc_277.htm]


Summary:

The Laurel Formation in the mapped area consists of sedimentary melange quartzofeldspathic matrix containing quartz "eyes" and fragments of meta-arenite, biotite schist, actinolite schist, and amphibolite. Upper part of unit contains more 50 percent olistoliths of meta-arenite and biotite schist. The Laurel is of Early Cambrian age.

Source: GNU records (USGS DDS-6; Reston GNULEX).


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For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

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